Land disturbance and recovery following a massive deforestation event in the Missouri Ozarks
Winston Crausaz
In 1983 California businessman Raymond L. Sheeks purchased 40 square kilometers of wooded upland in the Ozark Mountains of south-central Missouri. Starting with steep forested slopes, a relief of 100 meters, thin ...

Glacial Features of Franconia Notch, New Hampshire
R. Laurence Davis, University of New Haven
INTRODUCTION Franconia Notch, New Hampshire (Figure 1) is a classic northern Appalachian glaciated valley. It has geomorphic features from pre-glacial times, from the glaciation itself, from glacial meltwater, and ...

Cold climate conditions as a driver of alluvial fan deposition in the Lost River Range, Idaho, USA
Megan Kenworthy, Center for Ecohydraulics Research, University of Idaho, Boise
Numerous large alluvial fans sit along the western front of the Lost River Range (LRR) in east-central Idaho, USA (Figure 1). These alluvial fans form where streams exit confined basins within the mountain range, ...

Precipitation and debris flows in the Adirondacks
Devin McPhillips, University of Vermont
In the Adirondack Mountains in New York State, slide scars are distinctive features of the landscape. These scars are usually long, narrow exposures of bedrock on steeper slopes that form when debris flows scour ...

Human-Induced Floodplain Sedimentation in the Driftless Area of southwestern Wisconsin: Consequences on Riparian Ecosystems
Eric Booth, University of Wisconsin-Madison
The Driftless Area of southwestern Wisconsin (Figure 1) is a unique region in the Upper Midwest, USA, because it escaped the direct effects of continental glaciation. In contrast, surrounding areas have been ...

Development of Palimpsest Landscapes
Jasper Knight
In Physical Geography, a palimpsest landscape is one where, in any given region, the different landforms that make up the landscape are not of the same age, with some surface landforms being very young because they ...

Lightning as a Geomorphic Agent in Low-Latitude Mountains
Jasper Knight
It is often assumed that high mountain environments are dominated by the geomorphic imprints of cold-climate weathering and erosion processes, forming angular bedrock fragments that are commonly found across ...

Knickpoint migration and landscape evolution, Cullasaja River Basin, North Carolina
Sean Gallen, Colorado State University
Introduction: Localized high topographic relief, steep slopes, and frequent mass wasting — features commonly associated with tectonically active settings — characterize the landscapes of the southern ...

Defining rates of erosion using terrestrial cosmogenic nuclides in the Himalaya
Lewis Owen, North Carolina State University
The Himalaya and Tibet comprise the greatest mountain mass on our planet, stretching for ~ 2000 km east-west and >1500 km north-south with an average elevation of ~5000 m above sea level. The mountain mass ...

Fire geomorphology: Fire-related erosion helps to shape our landscapes
Kerry Riley
The frequency of large wildfires has increased on all vegetated continents (Bowman et al., 2009). Wildfires can have profound influences on erosion rates, particularly in steep mountain basins. Fire-related ...